First Data on the Age and P–T Formation Conditions of Zones of Low-Angle Dip Schistosity of the Belomorian Mobile Belt

The low-angle dip schistosity zones of the Belomorian mobile belt of northern Karelia are zones of plastic flow of thrust origin. They were formed from 1.85 to 1.90 Ga: 1879 ± 21 Ma according to 40 Ar/ 39 Ar for amphibole from amphibolites and 1857 ± 13 Ma according to the Sm–Nd isochron in amphibol...

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Published in:Doklady earth sciences 2018-05, Vol.480 (1), p.618-623
Main Authors: Kozlovskiy, V. M., Travin, V. V., Travin, A. V., Savatenkov, V. M.
Format: Article
Language:English
Subjects:
Amphiboles
Amphibolites
Earth and Environmental Science
Earth Sciences
Geochemistry
Isotopes
Magma
Metamorphic rocks
Metamorphism
Metamorphism (Geology)
Plastic flow
Plastics
Rocks
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Travin, V. V.
Travin, A. V.
Savatenkov, V. M.
description The low-angle dip schistosity zones of the Belomorian mobile belt of northern Karelia are zones of plastic flow of thrust origin. They were formed from 1.85 to 1.90 Ga: 1879 ± 21 Ma according to 40 Ar/ 39 Ar for amphibole from amphibolites and 1857 ± 13 Ma according to the Sm–Nd isochron in amphibolites. The P – T parameters of rock metamorphism in low-angle dip schistosity zones correspond to the boundary of amphibolite and granulite facies of metamorphism: T = 640–765°C, rarely rising to 826°C; P = 8.0–11.7 kbar. The hypothesis of the two-stage Paleoproterozoic metamorphism of rocks of the Belomorian mobile belt was introduced.
doi_str_mv 10.1134/S1028334X1805015X
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subjects Amphiboles
Amphibolites
Earth and Environmental Science
Earth Sciences
Geochemistry
Isotopes
Magma
Metamorphic rocks
Metamorphism
Metamorphism (Geology)
Plastic flow
Plastics
Rocks
title First Data on the Age and P–T Formation Conditions of Zones of Low-Angle Dip Schistosity of the Belomorian Mobile Belt
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